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Cheshire County is a county in the southwestern corner of the U.S. state of New Hampshire. As of the 2020 census, the population was 76,458. [1] Its county seat is the city of Keene. [2] Cheshire was one of the five original counties of New Hampshire, and is named for the county of Cheshire in England. It was organized in 1771 at Keene.
English: This is a locator map showing Cheshire County in New Hampshire. For more information, see Commons:United States county locator maps. Date: 12 February 2006:
The three-digit number is unique to each individual county within a state, but to be unique within the entire United States, it must be prefixed by the state code. This means that, for example, while Belknap County, New Hampshire is 001, Addison County, Vermont and Alachua County, Florida are also 001. To uniquely identify Belknap County, New ...
Gilsum is a town in Cheshire County, New Hampshire, United States. The population was 752 at the 2020 census. [2]
Chesterfield is a town in Cheshire County, New Hampshire, United States. The population was 3,552 at the 2020 census. [2] It includes the villages of Spofford and West Chesterfield. Chesterfield is home to Spofford Lake, Chesterfield Gorge Natural Area, and parts of Pisgah State Park and Wantastiquet Mountain State Forest.
Dublin Pond [1] or Dublin Lake is a 236-acre (0.96 km 2) [2] water body located in Cheshire County in southwestern New Hampshire, United States, in the town of Dublin.The pond lies at an elevation of 1,480 feet (451 m) above sea level, near the height of land between the Connecticut River/Long Island Sound watershed to the west and the Merrimack River/Gulf of Maine watershed to the east.
Richmond is a town in Cheshire County, New Hampshire, United States. The population was 1,197 at the 2020 census. [2] History.
On the weekend of October 8–9, 2005, parts of Alstead were devastated by a severe flood. Heavy rain in Cheshire County—at least 7 inches (180 mm) in a 30-hour period—caused the Cold River and its tributaries to swell. The streamflows, which were swollen by the surge of water from Warren Brook, exceeded a 500-year recurrence interval.